Permian Sea-level Changes and Rising-Falling Events in South China

WANG Cheng shan; LI Xiang hui; CHEN Hong de; QIN Jian xiong

Article Contents

Article Navigation > Acta Sedimentologica Sinica > 1999 > 17(4): 536-541

WANG Cheng shan, LI Xiang hui, CHEN Hong de, QIN Jian xiong. Permian Sea-level Changes and Rising-Falling Events in South China[J]. Acta Sedimentologica Sinica, 1999, 17(4): 536-541.

Citation:

WANG Cheng shan, LI Xiang hui, CHEN Hong de, QIN Jian xiong. Permian Sea-level Changes and Rising-Falling Events in South China[J]. Acta Sedimentologica Sinica, 1999, 17(4): 536-541.

Permian Sea-level Changes and Rising-Falling Events in South China

State key Laboratory of Oil/Gas Reservoir Geology and Exploitation,Sedimentary Geology Institute of Chengdu University,Chengdu 610059

Received Date: 1998-11-26
Rev Recd Date: 1999-01-02
Publish Date: 1999-12-10

Abstract

On the basis of sequence stratigraphy,fills and evolution of sedimentary basin,a primary research on the Permian sea level and eustatic changes,rise and fall events in South China have been studied in this paper. Eleven cycles of relative sea level rising falling,which is equal to the depositional sequences,are recognized in Permian in South China.Of them,two patterns of the relative sea level rising falling are distinguished out.The first is a change tendency of continuously slower rising→faster falling that is dominated in the Yangtze Craton,and the second is vice versa that is common in most parts of Cathayan Craton,especially in eastern shallow Cathayan Craton.The two patterns of relative sea level rising falling are just in symmetric tendency. Also the changing patterns of the second order eustasy are divided into “One and half" type and “Single" type through the Permian which are the representatives of Yangtze Craton and Cathayan Craton respectively.Here,the “One and half"type means that there are on complete second order cycle and less than half cycle in Permian in Yangtze Craton and western margin of the Cathayan Craton.And the “Single"type shows that there is just one complete rising falling cycle in the same period in the eastern shallow Cathayan Craton. There are five events of sea level rising and falling,i.e.,the rising event in early Qixia stage,the highest sea level stand event at the earliest Maokou stage,the lowest sea level stand event at the terminal Maokou stage,the rising event in primary Wujiaping stage,and the falling event at middle Changxing stage separately.It is proposed that most of the sea level rising and falling events are relevant to the regional tectonics superposed by the second eustasy. The patterns of sea level and eustatic changes are distinctly different from those in Euramerica.The time of the highest eustatic stand is aged as the earliest Maolou Stage,which approximately equals to the early Artinskian in Europe,to the early Leonardian in North America.But it is showed in the late Maolou Stage on the Vail Curve in 1977,and in the terminal Carboniferous in the Gondwana Land in the T R cycles by Ross and Ross in 1985.The lowest eustatic stand in the Yangtze Craton lies in the terminal Early Permian (latest Maokou Stage),but displays in earliest Permian on the Vil Curve (1977),and in latest Permian in the T R cycles by Ross and Ross in 1985.The total tendency of eustatic change in the Cathayan Craton is similar to that on the Vail Curve although the highest eustatic stand of the former formed earlier than the later.It is supposed that the controls are probably different in variable tectonic settings becaus the Yangtze Craton and western Cathayan Craton belong to the Tethyan tectonic field,and the eastern Cathayan Craton,Euramerica to the Pacific tectonic field.
- sea-level and eustatic change,
- sea-level rising -falling event,
- cause,
- Permian,
- South China

References

[1]

1 陈北岳, 颜佳新. 广西上二叠统层序地层格架 [J]. 地质科学,1994, 19(5):597～608

2 陈显群, 刘应楷, 童鹏. 东吴运动质疑及川黔运动之新见 [J]. 石油与天然气地质, 1987, 8(4):412～424

3 陈中强. 二叠纪末期的全球淹没事件 [J]. 岩相古地理, 1995, 15(3):34～39

4 胡世忠. 论东吴运动构造事件与二叠系分统界线问题 [J]. 地层学杂志, 1994, 18(4):309～315

5 田景春, 曾允孚. 中国南方二叠纪古海洋锶同位素演化 [J]. 沉积学报, 1995, 12(1):40～44

6 夏文臣, 周杰, 葛立刚等. 华南二叠 -三叠系的成因地层序列及古特提斯海重建 [J]. 地球科学, 1994, 19(5):663～675

7 肖文交, 李继亮, 何海清等. 浙西北前陆褶皱冲断带初步研究[J]. 中国科学(D 辑), 1997, 27(1):27～32

8 许效松, 刘宝王君, 赵玉光. 上扬子地台西缘二叠系 -三叠系层序地层界面成因分析与盆地转换 [J]. 特提斯地质(20), 1996:1～30

9 颜佳新, 方念乔. 湖北省栖霞组沉积环境、沉积旋回及层序地层划分 [J]. 地球科学, 1994, 19(5):620～625

10 杨美芳, 李继亮, 李红生等. 浙江长兴地区长兴组放射虫化石及其指相意义 [J]. 地质科学, 1997, 32(2):229～231

11 姚华舟, 张仁杰. 三峡地区二叠 -三叠系界线地层与地质事件[A]. 见:国家计委国土司和地矿部科技司主编, 地质科学研究论文集 [C]. 北京:中国经济出版社, 1997: 4～10

12 殷鸿福, 童金南, 丁梅华等. 扬子区晚二叠世 -中三叠世海平面变化 [J]. 地球科学, 1994a, 19(5):627～632

13 殷鸿福. 二叠、三叠系研究的进展 [J]. 地球科学进展, 1994b, 9(2):1～9

14 于炳松. 塔里木盆地北部石炭 -二叠纪高分辨率层序年代地层体制 [J]. 地质地球化学, 1996, 2:55～60

15 王立亭, 陆彦邦. 中国南方二叠纪岩相古地理与成矿作用 [M].北京:地质出版社, 1994:59～61

16 吴浩若, 邝国敦, 王忠诚. 广西晚古生代构造沉积背景的初步研究 [J]. 地质科学, 1997, 32(1):11～18

17 曾允孚, 刘文均, 陈洪德等. 华南右江盆地沉积构造演化 [M].北京:地质出版社, 1993. 1～15

18 赵金科. 华南晚二叠纪头足类. 古生物态(新乙种), 12 号, 1978

19 Ross C A, Ross J R P. Late Paleozoic deposi tional sequences aresynchronous and w orldw ide [J]. Geology, 1995, 13:194～197

20 Ross C A, Ross J R P. Lat e Paleozoic sea levels and deposit ional se-quences [A]. Cushman Foundation for Foraminiferal Research[C]. S pec. Publ., 1987, 24:137～149

21 V ai l P R, M itchm u R M Jr, Thompson S. Seismic St ratig raphy and global changes of sealevel [A]. In:Payt on C E ed. Sei smic S tratigraphy -Application t o Hydrocarbon Exploration [C]. AA PG,1984, 26:83～97

Proportional views

通讯作者: 陈斌, bchen63@163.com

1.
沈阳化工大学材料科学与工程学院沈阳 110142

Get Citation

PDF

XML

Article Metrics

Article views(589) PDF downloads(577) Cited by()

Proportional views

Permian Sea-level Changes and Rising-Falling Events in South China

State key Laboratory of Oil/Gas Reservoir Geology and Exploitation,Sedimentary Geology Institute of Chengdu University,Chengdu 610059

Received Date: 1998-11-26

Rev Recd Date: 1999-01-02

Publish Date: 1999-12-10

Key words:

Abstract: On the basis of sequence stratigraphy,fills and evolution of sedimentary basin,a primary research on the Permian sea level and eustatic changes,rise and fall events in South China have been studied in this paper. Eleven cycles of relative sea level rising falling,which is equal to the depositional sequences,are recognized in Permian in South China.Of them,two patterns of the relative sea level rising falling are distinguished out.The first is a change tendency of continuously slower rising→faster falling that is dominated in the Yangtze Craton,and the second is vice versa that is common in most parts of Cathayan Craton,especially in eastern shallow Cathayan Craton.The two patterns of relative sea level rising falling are just in symmetric tendency. Also the changing patterns of the second order eustasy are divided into “One and half" type and “Single" type through the Permian which are the representatives of Yangtze Craton and Cathayan Craton respectively.Here,the “One and half"type means that there are on complete second order cycle and less than half cycle in Permian in Yangtze Craton and western margin of the Cathayan Craton.And the “Single"type shows that there is just one complete rising falling cycle in the same period in the eastern shallow Cathayan Craton. There are five events of sea level rising and falling,i.e.,the rising event in early Qixia stage,the highest sea level stand event at the earliest Maokou stage,the lowest sea level stand event at the terminal Maokou stage,the rising event in primary Wujiaping stage,and the falling event at middle Changxing stage separately.It is proposed that most of the sea level rising and falling events are relevant to the regional tectonics superposed by the second eustasy. The patterns of sea level and eustatic changes are distinctly different from those in Euramerica.The time of the highest eustatic stand is aged as the earliest Maolou Stage,which approximately equals to the early Artinskian in Europe,to the early Leonardian in North America.But it is showed in the late Maolou Stage on the Vail Curve in 1977,and in the terminal Carboniferous in the Gondwana Land in the T R cycles by Ross and Ross in 1985.The lowest eustatic stand in the Yangtze Craton lies in the terminal Early Permian (latest Maokou Stage),but displays in earliest Permian on the Vil Curve (1977),and in latest Permian in the T R cycles by Ross and Ross in 1985.The total tendency of eustatic change in the Cathayan Craton is similar to that on the Vail Curve although the highest eustatic stand of the former formed earlier than the later.It is supposed that the controls are probably different in variable tectonic settings becaus the Yangtze Craton and western Cathayan Craton belong to the Tethyan tectonic field,and the eastern Cathayan Craton,Euramerica to the Pacific tectonic field.

HTML

Reference (1)

[1]

Permian Sea-level Changes and Rising-Falling Events in South China

Abstract

References

Proportional views

通讯作者: 陈斌, bchen63@163.com

Article Metrics

Proportional views

Related